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recipe for a weather forecast
initial conditions
data assimilation
numerical weather prediction
interpretation
chaos in modeling
atm. is a chaotic fluid
approximate present does not approximately determine future
Lorenz equations
system of 3 equations for a position of a particle in a space
describes chaotic behavior of a particle
limit of prediction
deterministic limit is 2 weeks
set by chaos + uncertainty of the initial condition
model grid
atm. divided into grid cells
laws of physics evaluated for each cell in horizontal + vertical direction
explicit resolution
for scales larger than the grid scale
parameter
represent sub-grid effects/phenomenons
contribute error to forecasts
data assimilation
process where observations are put into a model to generate initial conditions
takes observations
moves background field toward observations
background field
short-term forecast from previous run of model
ensemble
set of forecasts from slightly different starting conditions
where most weather predictions come from
reliable forecast
observed frequency matches predicted frequency
probabilistic forecast
predicts climate not specific weather
cloud formation
around condensation nuclei from cooling + condensing
types of cloud formation
air rising from solar heating
air pushed up over mountains
air lifted over a weather front
atmospheric stability
weather saturated air can freely rise
low clouds
stratus
cumulus
stratocumulus
cumulonimbus
medium clouds
nimbostratus
altostratus
altocumulus
high clouds
cirrus
cirrostratus
cirrocumulus
warm front
boundary between cold air ahead of front + warm air behind front
associated with rain
clouds + climate
high clouds trap more heat ↑ T
low clouds reflect more sunlight ↓ T
climate
statistical distribution of weather over decades
what changes impact of extreme weather
time
climate
conditions leading up to the event
initial conditions
UK heatwave
T exceeds a regionally-varying threshold > 3 days
tropical cyclones
classified based on sustained wind speeds
cyclone cone of uncertainty
shows avg. uncertainty, typical error of forecast based on the past 5 years
supercells
intense, rotating thunderstorms under which tornadoes form
requires unstable atm. + wind shear
in-situ atm. sensing
weather stations
buyos
weather balloons
aircraft
remote atm. sensing
radar
satellite
measuring T
through Stevenson screens
ground vs. air temp
hygrometer
humidity measuring device
relative humidity
actual water vapor/water vapor at sat.
dew point
T when air becomes fully sat. when cooled
wet bulb T
T of air becomes fully sat. when colled
absolute humidity
total water vapor in air
anemometer
measures wind @ 10 m
pyroheliometers
measures sunshine
radiosondes
weather balloons
only launched over land
satelite imagery for weather
visible
IR → cloud height
water vapor → wavelengths absorbed by water
geostationary satellites
orbit @ same speed as earth
show evolution of weather systems
polar orbiting satellites
orbit close to earth
orbit 1 time daily